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砂土液化不变性理论

CHEN Guoxing WU Qi Charng Hsein JUANG

防灾减灾工程学报2025,Vol.45Issue(6):1311-1370,60.
防灾减灾工程学报2025,Vol.45Issue(6):1311-1370,60.DOI:10.13409/j.cnki.jdpme.20250501002

砂土液化不变性理论

Invariance Theory of Sand Liquefaction under Cyclic Loadings

CHEN Guoxing 1WU Qi 1Charng Hsein JUANG2

作者信息

  • 1. Institute of Geotechnical Engineering,Nanjing Tech University,Nanjing 210009,China||Civil Engineering and Earthquake Disaster Prevention Center of Jiangsu Province,Nanjing 210009,China
  • 2. Emeritus College,Clemson University,SC 29634,USA
  • 折叠

摘要

Abstract

Due to the uncertainties in seismic motions and storm waves,the diversity of liquefiable soils,and the complexity of sand liquefaction mechanisms,fundamental issues such as fundamental physico-mechanical mechanisms behind excess pore water pressure(ue)generation in a liquefiable soil,the collective effects of multifactorial interactions on ue generation,and liquefaction triggering criteria remain unclear.Based on decades of studies,Chen et al.proposed an invariance theory of sand lique-faction,incorporating invariant state thresholds and intrinsic laws governing cyclic behavior and solid-liquid phase-transitions,which lead to a universal paradigm for site liquefaction evaluation rooted in in-variant physical and mechanical correlations.This novel theory of sand liquefaction mainly includes the following four aspects.(1)For a liquefiable soil at a specific initial physical state,the threshold general-ized shear strain is an intrinsic index that distinguishes nonlinear elastic and elastoplastic states,with a constant value.A power-law relationship is observed between cumulative dissipated energy per unit volume(Wc)and generalized shear strain amplitude(γga),reflecting the invariance in constitutive be-havior.(2)The evolution of soil particle-fabric system governs ue generation in liquefiable soils through physico-mechanical mechanisms,with physical state changes serving as the intrinsic mecha-nism driving ue generation.Differences in ue generation rates under various cyclic loadings primarily stem from corresponding differences in shear strain rates.The marginal peak excess pore pressure ratio(ru,pm),marking the transition from a solid-liquid mixed phase to a transiently viscous fluid phase,ex-hibits dual invariance in mechanics and physics.A ru,pm value of 0.90 can be used as a liquefaction trig-gering criterion for soils both in laboratory element tests and field conditions.The relationship between USR(unit cyclic stress ratio)and Nclt(number of cycles required to trigger liquefaction defined by ru,pm=0.90)follows a negative power-law,thereby forming the threshold state line between the solid-liq-uid mixed phase and the liquid phase.This USR-Nclt curve depends solely on the initial state of the soil.(3)The equivalent skeleton void ratio(e*sk)serves as a single-variable proxy for the physical state of granular soils.For soils with fines particle content below a threshold,negative power-laws exist in the correlations between liquefaction resistance(CRR15 or URR15)in 15 cycles and e*sk,and between the stress-corrected shear-wave velocity(Vs1)and e*sk.Based on the principle of mapping transitivity,a unique correspondence between CRR15 and Vs1,i.e.,liquefaction triggering curve,can be established through the index e*sk,indicating a novel and universal paradigm for site liquefaction potential evalua-tion.(4)The generalized shear strain serves as an equivalent shear strain(γeq)proxy for reflecting the 2D and 3D stress-strain state.A shear strain reversal at the irregular stress-strain loops of cycles in the Chen et al.'s generalized non-Masing,nonlinear,and hysteretic constitutive model of soil will occur when the incremental shear strain Δγeq=0.This strain reversal criterion is independent of the stress-strain hysteretic paths.The physical correlation between the maximum shear modulus and the extreme(maximum and minimum)void ratios exhibits an invariant mathematical form.Equivalent secant shear modulus and damping ratio across a wide strain range can be calculated through the shear stress/strain autocorrelation/cross-correlation functions,with algorithms invariant in mathematical form and physi-cal mechanism.The physics-based model for the peak pore pressure increment(Δuep)demonstrates tri-ple invariance in constitutive behavior,mathematical form,and cyclic loading conditions.A universal correlation links the peak pore pressure ratio(rup)to γga.The coupling of the Chen et al.'s non-Masing constitutive model and the Chen et al.'s Δuep model yields a novel effective stress-strain constitutive model of soil.Consequently,two novel universal site liquefaction potential evaluation methods are es-tablished:a total stress method(rup model-based)and an effective stress method(Δuep model-based).The invariance theory provides a unified basis for refining liquefaction mechanisms,improving evalua-tion methodologies,and advancing mitigation strategies in geotechnical earthquake engineering.The insights derived from decades of research,as reported in this study,will potentially enable the scientif-ic and engineering communities to reinterpret the liquefaction mechanism,its evaluation paradigms,and liquefaction mitigation strategies.

关键词

砂土液化/不变性理论/液化机理/固-液相变/液化触发准则/等效状态理论/场地液化评价范式

Key words

sand liquefaction/invariance theory/liquefaction mechanism/solid-liquid phase transition/liquefaction triggering criterion/equivalent state theory/site liquefaction evaluation para-digm

分类

建筑与水利

引用本文复制引用

CHEN Guoxing,WU Qi,Charng Hsein JUANG..砂土液化不变性理论[J].防灾减灾工程学报,2025,45(6):1311-1370,60.

基金项目

国家自然科学基金项目(52278503,52378346)资助 (52278503,52378346)

防灾减灾工程学报

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